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861.
Jufeng Zheng Xuhui Zhang Lianqing Li Pingjiu Zhang Genxing Pan 《Agriculture, ecosystems & environment》2007,120(2-4):129-138
Impacts of nutrient management on C mineralization and greenhouse gas (GHGs) emission from soils have been of much concern in global change. Using laboratory incubation, the production of CH4 and CO2 were studied from both bulk samples and the particle size fractions (PSF) of topsoil from a paddy under a long-term different fertilization trial (including non (NF), chemical without (CF) and with manure (CFM) fertilization, respectively) in the Tai Lake Region, China. Four PSFs (2000–200, 200–20, 20–2, <2 μm) were separated from undisturbed samples collected after rice harvest by a low-energy ultrasonic dispersion procedure. Both the bulk samples and PSFs were incubated under submerged condition for 72 days. The concentration of CH4 and CO2 evolved during incubation were determined by gas chromatography. C mineralization rates ranged from 0.13 to 0.52 mg C g−1 C day−1, with different fertilizations and size of the PSFs, and were not correlated with C/N ratio. While CO2 production predominated over CH4 from C mineralization from both bulk samples and the size fractions, CH4 production played a predominant role in the total global warming potential (GWP) under all treatments. C mineralization of bulk soil was significantly higher under CF than under CFM and NF. CH4 production, however, was 3 times as under CFM and 27 times as under NF, indicating a tremendous effect of chemical fertilization alone on the total GWP. CO2 production from the PSFs differed from CH4 under a single treatment, which was notably from the coarse PSFs larger than 200 μm. Higher C mineralization and CH4 production with a higher metabolic quotient under CF implicated a vulnerability of soil functioning of GHGs mitigation in the paddy receiving chemical fertilizers only. Thus, rational organic amendments should be undertaken for mitigating the climate change. 相似文献
862.
土壤中14 C 甲磺隆的可提取态残留物随时间延长不断降低 ,而其结合态残留率第 2 8天达最高 .14 C 甲磺隆结合态残留物在土壤腐殖物质中的分布是 :富啡酸 胡敏素 >胡敏酸 .在处理最初 2 8天 ,富啡酸中14 C 甲磺隆结合态残留物不断增大 ,随后减少 ;胡敏素中的结合态残留量在 2 8— 2 2 4天变化不大 .14 C残留物在不同土壤之间的结合及其分布都是有差异的 ,与土壤pH值、粘粒矿物类型等都有密切关系 相似文献
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865.
Yang Yang Xiuzhen Zheng Wei Ren Jiafang Liu Xianliang Fu Sugang Meng Shifu Chen Chun Cai 《Frontiers of Environmental Science & Engineering》2022,16(11):137
- Content>● Systematic information of recent progress in photocatalytic NO x removal is provided. Content>
- Content>● The photocatalysts with special morphologies are reviewed and discussed. Content>
- Content>● The morphology and photocatalytic NO x removal performance is related. Content>
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